18 Steele Street
18 Steele Street, Hackett ACT 2602, Australia
Sales history
| Event | Date | Price | Price per m² |
|---|---|---|---|
| Sold | Mar 2012 | $590,000 | $845 |
Price per m² based on land size of 698 m².
Key details
- Locality
- Hackett
- State
- ACT
- GNAF PID
A unique ID for this address in Australia's national address database.
- GAACT714884269
- Legal parcel ID
The official land parcel identifier used on property titles and plans.
- CANB/HACK/13/26
- Remoteness area
- Metro
- Property type
- House
- Land size
- 698 m²
- Internal area
- -
- Land Use Category
What the land is mainly used for, such as Residential, Commercial, Industrial or Other.
- Residential
Real Estate Agencies
Nearby schools
Frequently asked questions
How many bedrooms and bathrooms does 18 Steele Street have?
The house offers three bedrooms and two bathrooms, providing ample accommodation for families or sharing arrangements.
What is the size of the land parcel for this property?
The residence sits on a 698 m² block, giving space for a garden, outdoor entertaining or potential extensions.
How far is Hackett from Canberra’s central business district?
Hackett lies about 4.5 km north‑east of the Canberra CBD, making it a short drive or bike ride to the city centre.
What parks or recreational spaces are nearby?
Within a kilometre you’ll find Calvert Park (≈0.5 km), Dickson District Playing Fields (≈0.9 km), Bill Pye Park (≈1.2 km) and the nearby Mount Majura Nature Reserve to the east.
Which community facilities are close to the property?
St Margaret’s Uniting Church is just 0.4 km away, the Dickson Library is about 1.8 km distant, and the Ibis Styles Canberra Tall Trees hotel is roughly 1.7 km from the house.
Is there a bus shelter or public transport stop nearby?
The Officer Crescent bus shelter is approximately 1.1 km away, providing convenient access to local bus routes.
What geological features are characteristic of the Hackett area?
Hackett sits on calcareous shales from the Canberra Formation overlain by Quaternary alluvium, with the eastern side resting on the lowest layer of the Ainslie Volcanics, a grey dacite and associated volcanic material.